<<

(Ursus maritimus): Southern Beaufort Stock

STOCK DEFINITION AND GEOGRAPHIC RANGE

Polar bears are found throughout the circumpolar and occur in 19 subpopulations

(http://pbsg.npolar.no/en/status/; Obbard et al. 2010), also known as stocks (Figure 1). Polar bear ranges are extensive and individual activity areas can be large (up to 167,000 km2) (Garner et al.

1990, Amstrup et al. 2000). Six polar bear stocks have ranges extending into two or more countries (Amstrup et al. 1986, Amstrup and Demaster 1988, Obbard et al. 2010). Two polar bear stocks occur in , the Southern (SBS) and the Chukchi/Bering

(CBS) stocks (Figure 1). Together, the two stocks range throughout the Beaufort and Chukchi

Seas, including the nearshore habitats. The stocks overlap seasonally in the eastern Chukchi and western Beaufort Seas. The SBS stock is managed by the and and is also referred to as the Southern Beaufort Sea subpopulation when described by the International

Union for Conservation of Nature, Polar Bear Specialists Group (IUCN- PBSG; Aars et al.

2006).

The distinction between the SBS and CBS stocks was originally determined by: (a) movement information collected from capture-recapture studies of adult female bears (Lentfer

1983); (b) physical oceanographic features that segregate stocks (Lentfer 1974); (c) morphological characteristics (Manning 1971; Lentfer 1974; Wilson 1976); and (d) variations in

1 levels of heavy metal contaminants of organ tissues (Lentfer 1976, Lentfer and Galster 1987).

An extensive area of overlap between the Southern Beaufort Sea stock and the

Chukchi/Bering seas stock occurs between and Point Hope, centered near Point

Lay (Garner et al. 1990, Garner et al. 1994, Amstrup 2000, Amstrup et al. 2000, 2001a, 2002,

2004, 2005). Telemetry data indicates that adult female polar bears marked in the Southern

Beaufort Sea spend about 25% of their time in the northeastern , whereas females

captured in the Chukchi Sea spend only 6% of their time in the Southern Beaufort Sea (Amstrup

1995).

Despite their overlap in ranges (Figure 2) and uncertainty in the exact delineation, the

existence of two stocks is further supported by more recent information on contaminants (Evans

2004a, b; Kannan et al. 2007), movement data from satellite-linked collars (Garner et al. 1994,

Amstrup et al. 2004, 2005), and population responses to loss (Rode et al. 2014).

Additionally, very few bears in the CBS stock are observed denning within the range of the SBS

stock (Rode et al. 2015), and similarly, very few bears in the SBS stock are observed denning in

the range of the CBS stock (Durner et al. 2010).

Contaminants

Mercury (Hg), selenium (Se), and cadmium (Cd) concentrations in polar bear liver and kidney tissues were significantly higher in the SBS stock than in the CBS (Evans 2004a, Kannan et al. 2007, Routti et al. 2011), while the concentration of vanadium (V) in kidney tissue was higher in the CBS stock than in the SBS (Evans 2004a). In addition, Kannan et al. (2007) reported concentrations of trace elements of silver (Ag), bismuth (Bi), barium (Ba), copper (Cu), and tin 2 (Sn) were significantly higher in the CBS stock than the SBS stock.

In a separate study, Evans (2004b) analyzed the persistence of organochlorine (OC)

contaminants, including polychlorinated biphenyls (PCB) congeners;

dichlorodiphenyltrichloroethane (DDT) and its metabolites, including

dichlorodiphenyldichloroethylene (DDE); and chlordane-related compounds (CHL) in polar

bears from both stocks. While concentrations of OCs in the SBS and CBS stocks were relatively

low compared to other polar bear stocks, concentrations of OCs were higher in the SBS than in

the CBS stock. Dietz et al. (2015) also found that concentrations of organohalogen contaminants

exceeded a toxic effect threshold for bears in Alaska, although the levels found there were the

lowest of the stocks considered. Similarly, McKinney et al. (2011) found that polar bears in

Alaska tended to have higher levels of DDT contamination than other .

Genetics

Several modern studies have investigated the genetics of polar bears throughout their range.

Analysis of mitochondrial DNA and microsatellite DNA loci indicates little differentiation between the SBS and CBS polar bear stocks (Cronin et al. 1991, 2006, Scribner et al. 1997). Using 16 variable microsatellite loci, Paetkau et al. (1999) observed small differences in genetic distances between the SBS stock and CBS stock; however, a lack of dramatic genetic variation led researchers to conclude that polar bears belong to a single evolutionary significant unit. More recently Peacock et al. (2015) and Malenfant et al. (2016) characterized genetic structure of polar bears subpopulations into large clusters. Peacock et al. (2015) identified four clusters, and

Malenfant et al. (2016) identified six clusters, with the SBS and CBS occupying the same cluster in 3 both studies. While genetically similar, demographic and movement data indicate a degree of site fidelity, suggesting that the stocks should be managed separately, while recognizing that delineation of the CBS and SBS stocks includes a of overlap (Amstrup 2000, Amstrup et al.

2000, 2001, 2002, 2004, 2005).

Distribution

The SBS polar bear stock is distributed predominantly throughout the central Beaufort

Sea region. The western edge of their range is near Icy Cape, although the exact boundary between the SBS and the CBS stocks is uncertain. Amstrup et al. (2000) reported that the eastern boundary of the Southern Beaufort Sea stock occurred south of and east of the Baillie Islands, Canada. However, analysis of polar bear movements using satellite telemetry from 2000 to 2006 (Amstrup et al. 2004, 2005), capture-recapture data (Regehr et al. 2006,

Stirling et al. 2007), and harvest information suggest the eastern boundary for the SBS stock may be more appropriately located further west, near the village of , Canada.

Responses to Changing Sea Ice Conditions

In response to changes in sea ice characteristics and declines in sea ice habitat over the during the summer and late autumn (Stroeve et al. 2014), some polar bears of the SBS stock have shifted their ranges to search for seals on ice and to access the remains of subsistence-harvested bowhead whales on land (Schliebe et al. 2008, Atwood et al. 2015a).

Changes in distribution and movements, including increased land use during the summer, are expected to occur with increasing frequency in the future (Durner et al. 2009, Amstrup et al.

4 2007, Schliebe et al. 2008, Atwood et al. 2015a) and could lead to greater levels of human-polar bear conflict. Changing sea ice conditions have also led to more frequent observations of long- distance swims by polar bears in the SBS stock with the potential for significant energetic costs and impacts to survival (Durner et al. 2011, Pagano et al. 2012).

In addition, polar bears from the SBS stock have historically denned on both the sea ice and land, but thinning of sea ice in recent years may have contributed to a decline in the proportion of polar bears denning on the sea ice. Fischbach et al. (2007) found that the proportion of dens on the pack ice declined from 62% during the period from 1985 to 1994 to

37% during the period from 1998 to 2004. Currently, the primary terrestrial denning areas for the SBS stock in Alaska occur on the barrier islands from Barrow to Kaktovik, and along coastal areas up to 25 miles inland, including the Arctic National Wildlife Refuge to Peard Bay, west of

Barrow (Amstrup and Gardner 1994, Amstrup 2000, Durner et al. 2001, 2006, 2013).

Polar bears are generally expected to experience nutritional stress as loss of Arctic sea ice continues (e.g., Stirling and Parkinson 2006, Amstrup et al. 2010, Rode et al. 2010). In some regions ice loss has apparently led to negative demographic effects (Regehr et al. 2007, 2010,

Bromaghin et al. 2015), while in other regions polar bear subpopulations appear stable or increasing (Stirling et al. 2011, Peacock et al. 2013, Rode et al. 2014). In a recent study, Rode et al. (2014) found that SBS stock bears were responding differently to changing sea ice conditions compared to bears in the CBS stock. During the period from 2008 to 2011, bears inhabiting the

Chukchi Sea were in better condition, larger, and appeared to have higher reproductive rates than bears inhabiting the southern Beaufort Sea (Rode et al. 2014).

5 In another study investigating climate effects on bears, Hunter et al. (2010) used the relationships between sea ice and polar bear vital rates estimated during the period from 2001 to

2006 to project the long-term status of the SBS stock under sea ice conditions as forecast by global climate models. The projection suggested there could be a high probability of significant population decline in the 21st century for the SBS stock. More recently, Bromaghin et al. (2015) analyzed demographic data from 2001 to 2010, and found similar evidence to Regehr et al.

(2010) for expected low survival of all sex and age classes of polar bears in the mid-2000s.

However, Bromaghin et al. (2015) also found survival of most sex and age classes of polar bears

in the SBS stock increased during the period from 2007 to 2010, despite continued declines in

the availability of sea ice.

POPULATION SIZE

Polar bears occur on sea ice at low densities throughout much of their range (DeMaster and Stirling 1981). Accurate estimates of abundance for the SBS stock have been difficult to obtain because of low population densities, inaccessibility of habitat, movement of bears across management and international boundaries, and budget limitations (Amstrup and DeMaster 1988,

Garner et al. 1992). Research on the SBS stock began in 1967 and is one of only four polar bear subpopulations with long term (greater than 20 years) data.

Long term capture-recapture studies in the Beaufort Sea have provided several estimates of

abundance of the SBS stock; however, direct comparison may be inaccurate due to varied

sampling strategies and analyses. Amstrup et al. (1986) estimated abundance of the SBS stock to

be 1,778 bears during the period from 1972 to 1983. The abundance in 1992 was estimated at 6 1,480 animals (Amstrup (1995). In 2001, Amstrup (USGS, unpublished data) approximated an

abundance of 2,272 bears based on an estimate of 1,250 females and a sex ratio of 55% females

(Amstrup et al. 2001b). In 2006, a capture-recapture study that sampled American and Canadian portions of the Beaufort Sea region from 2003 to 2006 estimated abundance of the SBS stock in

2006 to be 1,526 individuals (Regehr et al. 2006). A subsequent capture-recapture analysis during the period from 2004 to 2010 suggested a reduction in survival and abundance from 2004 through 2007 and subsequently, the population appeared to stabilize with improved adult and cub survival (Bromaghin et al. 2015). From this analysis they calculated an abundance estimate of approximately 900 bears in 2010 (Bromaghin et al. 2015). Possible negative biases in abundance estimates may exist due to variation in the intensity and geographic coverage of capture-

recapture sampling (specifically, a lack of systematic sampling in some portion of the stock’s

Canadian range during the period from 2007 to 2010; Bromaghin et al. 2015). Thus, such

possible negative biases necessitate a cautious interpretation of trends and point estimates of

abundance for the SBS stock. Conservatively, the decline in abundance of the SBS stock seemed

unlikely to have been less than 25%, but may have approached 50% (Bromaghin et al. 2015).

Abundance estimates in Bromaghin et al. (2015) and previous analyses were based on capture- recapture sampling that ended at Barrow and did not extend farther west to where some polar bears from the SBS stock may be found. Data collection is ongoing and updated population

estimates are expected in the future.

Minimum Population Estimate

Under the Protection Act of 1972, as amended (MMPA), a “minimum 7 population estimate” (NMIN) is defined as “an estimate of the number of animals in a stock that is based on the best available scientific information on abundance, incorporating the precision and variability associated with such information; and provides reasonable assurance that the stock size is equal to or greater than the estimate.”

For polar bears in the SBS stock, the most recent population estimate is approximately

900 animals in 2010, based on analysis of data during the period from 2001 to 2010 (Bromaghin

th et al. 2015). The corresponding NMIN is calculated based on the lower 20 percentile of the sampling distribution for population size, using the methods of Wade (1998), as follows: NMIN =

N/exp(0.842 * (ln(1+CV(N)2))½) = 782 animals, where N = 900 animals and the coefficient of variation (CV) = 0.17 (Bromaghin et al. 2015).

This estimate may be biased low because the western extent of the study area (Point

Barrow) fell short of the SBS stock range, which extend west of Point Barrow to Icy Cape

(Obbard et al. 2010).

Current Population Trend

Although no quantitative information is available to estimate population status prior to

8 the 20th century, polar bear harvest during that period was largely conducted by Alaskan Natives

for subsistence (Schliebe et al. 2006), and the stock is, therefore, believed to have existed at or

near its environmental carrying capacity. Harvest by non-Alaska Natives became common in the

early 1960s, and the size of the stock declined substantially (Amstrup et al. 1986, Amstrup

1995). Sport harvest in Alaska was eliminated after passage of the MMPA in 1972, and the SBS

stock increased in numbers for the following 20 years. This increase was based on: (a) capture-

recapture data; (b) observations by Alaska Natives and residents of coastal Alaska;

(c) live-capture of polar bears per unit effort indices (USGS unpublished data); and (d) harvest statistics. Additionally, recapture data from the SBS stock indicated a population growth rate of

2.4% from 1981 to 1992 (Amstrup 1995).

However, the SBS stock experienced little or no growth during the 1990s (Amstrup et al.

2001b). Evidence suggests that SBS stock experienced negative effects from habitat loss due to . Declines in body size, body condition, and recruitment in recent decades have been associated with declining sea ice availability (Regehr et al. 2006, Rode et al. 2010, 2014).

Further, Regehr et al. (2010) suggested several years of reduced sea ice in the mid-2000s were

associated with low breeding probability and survival, leading to a negative population growth

rate.

Relationships between sea ice and polar bear population dynamics in the southern

9 Beaufort Sea are complex and likely reflect a combination of factors, such as ecological variation and density effects. Reduced spatial and temporal availability of sea ice is expected to be an increasingly important factor in population dynamics of SBS stock polar bears. As the climate continues to warm, polar bears will likely experience reduced access to prey, reduced cub survival, and deficient body condition. Based on all available data, the IUCN-PBSG considered the current trend of the SBS population to be in decline (PBSG 2015). The Service supports this determination.

CURRENT AND MAXIMUM NET PRODUCTIVITY RATES

Direct estimates of maximum net productivity rates (RMAX) are not available for the SBS

stock, although values can be inferred based on capture-recapture studies in the region and

knowledge of polar bear population dynamics. The following information was used to estimate

RMAX. During the period from 1981 to 1992 the population of SBS stock was increasing and

vital rates of polar bears were as follows: average age of sexual maturity (females) was 6.0 years;

average cub of year (COY) litter size was 1.7; average reproductive interval was 3.7 years; and

average annual natural mortality ranged from 1.0-3.0% for adult age classes (Amstrup 1995).

Using these data, Amstrup (1995) projected an annual intrinsic growth rate (i.e., natural mortality excluding human-caused mortality) of 6.0% for the SBS stock. More recently, survival and reproductive rates for the SBS stock for the period from 2004 to 2006 (Regehr et al. 2010) indicated that, under favorable sea ice conditions, the population was capable of increasing

10 between 6.0% and 7.5% annually (Hunter et al. 2010). Because the SBS stock was not at a greatly reduced density when any of the preceding estimates were made, these estimates are likely lower than the maximum intrinsic growth rate for the population. For the purpose of this assessment, we use RMAX of 7.5% as the current net productivity rate for the SBS stock but acknowledge that potential current and future effects of sea ice loss could lead to lower realized growth rates (Regehr et al. 2010, 2015 Bromaghin et al. 2015).

POTENTIAL BIOLOGICAL REMOVAL (PBR)

The MMPA defines Potential Biological Removal (PBR) level as the product of the minimum population estimate of the stock, one-half the maximum theoretical or estimated net productivity rate of the stock at a small population size, and a recovery factor (FR) of between

0.1 and 1.0: PBR = NMIN X 0.5RMAX X FR. Wade and Angliss (1997) recommend a default recovery factor (FR) of 0.5 for a threatened population or when the status of a population is

unknown. Therefore, we have calculated a PBR of 14 bears per year for the SBS stock using a

NMIN of 782, a RMAX of 7.5%, and a FR of 0.5.

ANNUAL HUMAN CAUSED MORTALITY AND SERIOUS INJURY

Fisheries Information

Polar bear stocks in Alaska have no direct interaction with commercial fisheries activities. Consequently, the total fishery mortality and serious injury rate for the SBS stock is

11 zero.

Total Mortality

1. Native Subsistence Harvest

Alaska Natives have hunted polar bears for subsistence purposes for centuries (Lentfer

1976), and polar bears continue to be an important resource for the Inupiat and Yupik peoples of coastal communities throughout northern and western Alaska (Brower et al. 2002, Johnson

2002). Polar bears provide a source of meat and raw materials for clothing and handicrafts, and polar bear hunting is a source of pride, prestige, and accomplishment for Native hunters.

Although polar bear hunting was prohibited by the MMPA in 1972, an exemption was made for

Alaska Natives living in coastal communities to allow them to hunt polar bears for subsistence

purposes and for the creation and selling of authentic native articles of handicraft and clothing,

provided that take was not accomplished in a wasteful manner.

For the SBS stock, subsistence harvest is addressed through an agreement between the

Inuvialuit of Canada and the Inupiat of Alaska (I-I Agreement; Brower et al. 2002). In 2010,

Commissioners of the I-I Agreement recommended that the combined U.S.-Canada quota be reduced from 80 bears to 70 bears, shared equally between the countries (USFWS 2011).

Subsequently, in Canada, the boundary of the SBS stock with the neighboring Northern

Beaufort Sea (NBS) stock was adjusted through polar bear management by-laws in the

Inuvialuit Settlement Region in 2013, affecting Canadian quotas and harvest levels from the

SBS stock, the current subsistence harvest of 56 bears total (35 in the United States and 21 in

Canada) reflect this change. For the most recent 10-year period, 2006-2015, an average of 19 12 bears per year were removed from the U.S. portion of the SBS stock (see Figure 3, which provides the annual estimated removals above each graph bar). The average sex composition of removals during this period was 27% female, 50% male, and 23% unknown. During the same time period the average Canadian harvest for the SBS was 14.2 bears per year with a sex ratio of

56 males to 44 females.

2. Other Mortality

Other forms of bear removals include those associated with accidental mortality during scientific research, during industrial activities, defense of life, and placement of orphaned cubs.

Two research-related mortalities have occurred between 2005 and 2015. One removal occurred in 2005 and the other removal happened in 2009. Two mortalities occurred as a result of deterrence activities. In 2011, a bear was killed during a deterrence action by an oil and gas company. In 2012, another bear was killed during a deterrence action by a village bear patrol.

Under section 109(h) of the MMPA, orphaned cubs can be removed from the wild and maintained in a facility for the protection or welfare of the cub. Such a situation occurred in 2011, when an orphaned cub was removed from the Beaufort Sea coast and placed into a long-term care facility that has cooperative agreement with the Service, after it was discovered near an industrial facility.

In 2012, one adult female and her two-year old male cub were found dead on an island

in northern Alaska. The true cause of their deaths remains unknown.

13 In 2014, two defense-of-life mortalities by non-Alaska Natives occurred with humans

engaged in recreational activities. The first incident occurred in August 2014 at Bullen Point and

the second occurred a week later in the Arctic National Wildlife Refuge.

STATUS OF STOCK

On May 15, 2008 (73 FR 28212), the Service listed all polar bears across their range as

“threatened” under the Endangered Species Act of 1973, as amended (ESA). Due to this listing under the ESA, the polar bear is considered “depleted” under the MMPA, and the SBS stock is considered to be a strategic stock under the MMPA.

OTHER FACTORS THAT MAY BE CAUSING A DECLINE OR IMPEDING RECOVERY OF THE STOCK

1. Climate Change

Climate change has been identified as the primary threat facing polar bear populations, with the SBS stock occurring in an ecoregion with a high probability of becoming greatly decreased by mid-century (Atwood et al. 2016). Polar bears are adapted to life in a sea ice environment. They depend on the sea ice-dominated ecosystem to support essential life functions. Sea ice provides a platform for hunting, denning, feeding, and resting; seeking mates and breeding; movement to terrestrial maternity denning areas; and long-distance movements (Stirling and Derocher 2012).

The sea ice ecosystem supports ringed seals (Phoca hispida), the primary prey for polar bears, and other marine mammal prey (Thiemann et al. 2008, Rode et al. 2014). In 2012, the National Marine

Fisheries Service (NMFS) listed two prey species of polar bears, the Arctic subspecies of (Phoca hispida hispida) and the Beringia distinct population segment (DPS) 14 (Erignathus barbatus nauticus), as threatened species under the ESA (77 FR 76706 and 77 FR

76740; December 28, 2012). Both species were listed due to climate change and declines in population of either or both of these important prey species may have deleterious impacts on polar bears.

Sea ice is rapidly diminishing throughout the Arctic (Stroeve et al. 2012) and large declines in polar bear habitat have occurred in the southern Beaufort and Chukchi Seas between the period from 1985 to 2006 (Durner et al. 2009). In addition, it is predicted that the greatest declines in

21st century polar bear habitat will occur in Chukchi and southern Beaufort Seas (Amstrup et al.

2007, Durner et al. 2009, Douglas 2010). Patterns of increased temperatures, earlier onset of and longer open water periods, later onset of freeze-up, increased rain-on-snow events, and potential reductions in snowfall are occurring. In addition, positive feedback systems (i.e., the sea-ice albedo feedback mechanism) and naturally occurring events, such as warm water intrusion into the Arctic and changing atmospheric wind patterns, can operate to amplify the effects of these phenomena. The following changes have been documented in the southern

Beaufort Sea: increased fragmentation of sea ice; an increase in the extent of open water areas seasonally; reduction in the extent and area of sea ice in all seasons; retraction of sea ice away from productive continental shelf areas during the summer; reduction of the amount of multi- year ice, and declining thickness and quality of shore-fast ice (Parkinson et al 1999, Rothrock et al. 1999, Comiso 2003, Fowler et al. 2004, Lindsay and Zhang 2005, Holland et al. 2006,

Comiso 2006, Serreze et al. 2007, Stroeve et al. 2008).

The SBS stock appears to be experiencing effects of changing sea ice conditions (Hunter

15 et al. 2010, Regehr et al. 2010, Rode et al. 2010, 2014, Bromaghin et al. 2015). Behaviorally, polar bears in the stock are have been observed shifting to greater use of land during later summer and autumn (Gleason and Rode 2009). Although relationships between sea ice and vital rates for polar bears are more complex than previously hypothesized (Bromaghin et al. 2015), sea ice loss and associated ecological changes are expected to have the greatest impact on SBS stock population dynamics, and long-term polar bear population declines are forecast if sea ice loss continues (Amstrup et al. 2007, Hunter et al. 2010). Traditional knowledge suggests that polar bears in the SBS stock may be getting smaller and changing denning patterns, potentially in relation to changing sea ice and climate conditions (Joint Secretariat 2015). The SBS stock appears to be vulnerable to large-scale, dramatic seasonal fluctuations in ice movements; decreased abundance and access to prey; and increased energetic costs of hunting. Hence, the

Service is working with multiple partners on measures to protect polar bears and their habitats.

2. Subsistence Harvest – Combined U.S. and Canada

Recognition that management of polar bears in the SBS stock is shared between Canada and Alaska led to the development of the Inuvialuit-Inupiat Agreement (I-I Agreement) between the Inuvialuit of the Inuvialuit Game Council, Canada, and the Inupiat of the North Slope

Borough, Alaska, in 1988 (I-I Agreement, Nageak et al. 1991, Treseder and Carpenter 1989,

Prestrud and Stirling 1994, Brower et al. 2002). During the period from 1988 to 2014 (the most current data), the combined Alaska and Canada mean harvest from the SBS stock has been approximately 56 bears per year (USFWS unpublished data). During the more recent time period (2006-2015), removals due to human causes have been lower (approximately 33 bears per 16 year in Alaska and Canada). The harvest in Canada is regulated by a quota system (Prestrud and

Stirling 1994, Brower et al. 2002), which has resulted in accurate harvest reporting, strict controls on harvest, and efficient monitoring and enforcement. Between July 2011 and June

2016, 90 bears were harvested in the Canadian portion of the SBS, below the quota of 143 bears.

The two most recently reported annual harvest in the Canadian portion of the SBS was 9 bears in

2014-2015 and 9 bears in 2015-2016; below the annual quota of 21 bears. The harvest quota established under the I-I Agreement in Alaska is voluntary and less efficient, overall, compared to the Canadian system (Brower et al. 2002).

Given the change of management boundary between the SBS and NBS stocks in Canada and evidence for population decline of the SBS stock (Bromaghin et al. 2015), harvest quotas should be reassessed to ensure harvest remains at a sustainable rate. Additionally, population data for the SBS stock need to be updated. The Service and its partners, including the North

Slope Borough and Inuvialuit Game Council, are currently conducting harvest risk analyses and working with stakeholders to identify potential adaptive management strategies for the SBS stock.

3. Oil and Gas Development

Oil and gas development and shipping occur within the range of SBS stock polar bears.

Increases in circumpolar Arctic oil and gas development, coupled with increases in shipping due to the lengthening open water season, increase the potential for an oil spill to negatively affect polar bears and their habitat. Oiled polar bears are unable to effectively thermoregulate, and may be poisoned by ingestion of oil during grooming (Øritsland et al. 1981) or eating contaminated 17 prey (St. Aubin 1990). In addition, polar bears can be attracted to petroleum products and actively investigate oil spills. They also are known to consume foods fouled with petroleum products (St. Aubin 1990; Derocher and Stirling 1991).

The Service works to monitor and mitigate potential impacts of oil and gas activities on polar bears through Incidental Take Regulations (ITRs), as authorized under the MMPA. Under these regulations, oil and gas activities must: 1) ensure impacts to small numbers of polar bears remain negligible, 2) minimize impacts to their habitats, and 3) ensure no unmitigable adverse impact on polar bear availability for Alaska Native subsistence use. The ITR program also requires monitoring and reporting to provide a basis for the evaluation of potential impacts of current and future activities on polar bears. The Service has concluded that at current levels, oil and gas exploration posed a relatively minor threat to the bears of the SBS stock (81 FR 52276;

August 5, 2016). Current ITRs for the southern Beaufort Sea region will expire in 2021.

While polar bears could be impacted by future onshore or offshore oil spills, historically the SBS

polar bear stock has not been impacted by oil spills in the Beaufort Sea. Between 1985 and 2013,

eight crude oil spills of amounts greater than 500 barrels occurred on the North Slope of Alaska,

within the range of the SBS stock (BOEM 2014). These spills posed little risk to polar bears and no impact to polar bears from the spills were documented because the spills occurred in heavily industrialized areas during times of the year when polar bear use was low. In addition, no offshore exploration wells have been drilled (an activity which would increase the risk of an offshore oil spill) in the Beaufort Sea since 2003 (BOEM 2014).

Nonetheless, oil spills remain a concern for polar bears throughout their range, especially

18 given the challenges of cleaning up spills in arctic waters (National Research Council 2014).

Polar bears are most vulnerable to oil spills during times when they aggregate near onshore food

resources, such as autumn polar bear aggregations near subsistence-harvested

carcasses at Point Barrow, Cross Island, and Kaktovik (76 FR 47010; August 3, 2011). Potential

impacts from an oil spill depend on the size, location, and timing of spills relative to polar bear

distributions; and also on the effectiveness of spill response and clean-up efforts. Bears could

also be affected indirectly either by food contamination or by chronic lasting effects caused by

exposure to oil (St. Aubin 1990).

Although the probability of an oil spill affecting a significant portion of Alaska’s polar bears

in the foreseeable future is low, we recognize that the potential impacts from such a spill

could be significant, particularly if subsequent clean-up efforts were ineffective. At present,

the Service is working with industry, oil spill response agencies, public display facilities, and

others to increase response capabilities for dealing with oiled or compromised bears in the

event of a spill. In addition, the Service has updated its polar bear oil spill response plan. This

plan is meant to help prepare and improve the Service’s response capabilities by describing

appropriate response strategies, clarifying response roles, obtaining the necessary training,

and improving our capability for holding and treating oiled bears.

4. Shipping

Loss of Arctic sea ice has resulted in an increase of open water, which, in turn, has led to an

increase in Arctic shipping. Given projections of an ice-free Arctic in summer months between

2020 and 2050 (Overland and Wang 2013) and an ice-free Arctic in the near future (Smith and 19 Stephenson 2013), the increase in shipping is expected to continue at a rapid pace.

Potential effects of shipping on polar bears include disturbance, increased fragmentation of sea ice habitat (from icebreakers), pollution, and the introduction of waste/marine litter (Polar Bear Range

States 2015). Increased vessel traffic will also increase the chances of an oil spill from a vessel sinking, a tanker accident, ballast discharge, or discharges during the loading and unloading of oil at ports.

CITATIONS

Aars, J., N.J. Lunn, and A.E. Derocher (Eds.). 2006. Polar bears: Proceedings of the 14th

working meeting of the IUCN/SSC Polar Bear Specialist Group, 20–24 June, Seattle,

Washington, USA. IUCN, Gland, Switzerland. 189 pp.

Amstrup, S.C. 1995. Movements, distribution, and population dynamics of polar bears in the

Beaufort Sea. Ph.D. Dissertation. University of Alaska-Fairbanks, Fairbanks, Alaska,

299 pp.

Amstrup, S.C. 2000. Polar Bear. In: J.C. Truett and S.R. Johnson (Eds.), The Natural History

of an Oil Field: Development and Biota (pp. 133–157). Academic Press, Inc., New York,

New York, USA.

Amstrup, S.C. and D.P. DeMaster. 1988. Polar bear, Ursus maritimus. In: J.W. Lentfer, (Ed.),

Selected Marine Mammals of Alaska: Species Accounts with Research and Management

Recommendations (pp. 39–45). Marine Mammal Commission, Washington, D.C.

Amstrup, S., and C. Gardner. 1994. Polar bear maternity denning in the Beaufort Sea. Journal

20 of Wildlife Management 58(1):1–10.

Amstrup, S.C., I. Stirling, and J.W. Lentfer. 1986. Past and present status of polar bears in

Alaska. Wildlife Society Bulletin 14:241–254.

Amstrup, S.C., G. Durner, I. Stirling, N.J. Lunn, and F. Messier. 2000. Movements and

distribution of polar bears in the Beaufort Sea. Canadian Journal of Zoology 78:948-966.

Amstrup, S.C., G.M. Durner, T.L. McDonald, D.M. Mulcahy, and G.W. Garner. 2001a.

Comparing movement patterns of satellite-tagged male and female polar bears. Canadian

Journal of Zoology 79:2147–2158.

Amstrup, S.C., T.L. McDonald, and I. Stirling. 2001b. Polar bears in the Beaufort Sea: A 30-

year mark-recapture case history. Journal of Agricultural, Biological, and Environmental

Statistics 6(2):221–234.

Amstrup, S.C., G.M. Durner, A.S. Fischbach, K. Simac, and G. Weston-York. 2002. Polar Bear

Research in the Beaufort Sea. In: N. Lunn, E. W. Born, and S. Schliebe (Eds.), Proceedings

of the 13th Working Meeting of the IUCN/SSC Polar Bear Specialist Group, Nuuk,

Greenland (pp. 109-125). IUCN, Gland, Switzerland, and Cambridge, U.K. vii + 153 pp.

Amstrup, S.C., T.L. McDonald, and G. Durner. 2004. Using satellite radiotelemetry data to

delineate and manage wildlife populations. Wildlife Society Bulletin 32(3):661–679.

Amstrup, S.C., G.M. Durner, I. Stirling, and T.L. McDonald. 2005. Allocating harvests among

polar bear stocks in the Beaufort Sea. Arctic 58:247–259.

Amstrup, S.C., Marcot, B.G. and Douglas, D.C. 2007. Forecasting the range-wide status of

polar bears at selected times in the 21st century. Administrative Report, US Geological

21 Survey. Reston, Virginia.

Amstrup, S.C., DeWeaver, E.T., Douglas, D.C., Marcot, B.G., Durner, G.M., Bitz, C.M., and

Bailey, D.A. 2010. Greenhouse gas mitigation can reduce sea-ice loss and increase polar

bear persistence: Nature. v. 468, no. 7326. pp. 955–958. doi:10.1038/nature09653.

Atwood, T.C., E.M. Peacock, M.A. McKinney, K. Lillie, R.R. Wilson, and S. Miller. 2015.

Demographic composition and behavior of polar bears summering on shore in Alaska.

U.S. Geological Survey Administrative report, Anchorage, Alaska.

Atwood, T.C., B.C. Marcot, D.C. Douglas, S.C. Amstrup, K.D. Rode, G.M. Durner, and J.F.

Bromaghin. 2016. Forecasting the relative influence of environmental and anthropogenic

stressors on polar bears. Ecosphere 7:e01370.

Bureau of Energy Management (BOEM). 2014. Alaska Outer Continental Shelf Chukchi

Sea Planning Area Oil and Gas Lease Sale 193 In the Chukchi Sea, Alaska Final Second

Supplemental Environmental Impact Statement, Volume 1. OCS EIS/EA BOEM 2014-

669.

http://www.boem.gov/uploadedFiles/BOEM/About_BOEM/BOEM_Regions/Alaska_Re

gion/Leasing_and_Plans/Leasing/Lease_Sales/Sale_193/2015_0127_LS193_Final_2nd_

SEIS_Vol1.pdf.

Bromaghin, J.F., T.L. McDonald, I. Stirling, A.E. Derocher, E.S. Richardson, D.C. Douglas,

G.M. Durner, T. Atwood, and S.C. Amstrup. 2015. Polar bear population dynamics in the

southern Beaufort Sea during a period of sea ice decline. Ecological Applications 25:634–

22 651.

Brower, C.D., A. Carpenter, M. Branigan, W. Calvert, T. Evans, A. Fischbach, J. Nagy, S.

Schliebe, and I. Stirling. 2002. The polar bear management agreement for the southern

Beaufort Sea: An evaluation of the first ten years of a unique conservation agreement.

Arctic 56:362-372.

Comiso, J.C. 2003. Warming trends in the Arctic from clear sky satellite observations. Journal

of Climate 16:3498-3510.

Comiso, J.C. 2006. Arctic warming signals from satellite observations. Weather 61(3):70–76.

Cronin, M.A., S.C. Amstrup, G.W. Garner, and E.R. Vyse. 1991. Interspecific and intraspecific

mitochondrial DNA variation in North American bears (Ursus). Canadian Journal of

Zoology 69:2985–2992.

Cronin, M.A., S.C. Amstrup, and K.T. Scribner. 2006. Microsatellite DNA and mitochondrial

DNA variation in polar bears (Ursus maritimus) in the Beaufort and Chukchi seas,

Alaska. Canadian Journal of Zoology 84:655–660.

DeMaster, D.P., and I. Stirling. 1981. Ursus maritimus. Mammalian Species:1-7.

Derocher, A.E., and I. Stirling. 1991. Oil contamination of two polar bears. Polar Record

27:56–57.

Dietz, R., K. Gustavson, C. Sonne, Desforges J.P., F.F. Rigét, V. Pavlova, M.A. McKinney, R.J.

Letcher. 2015. Physiologically-based pharmacokinetic modelling of immune, reproductive

and carcinogenic effects from contaminant exposure in polar bears (Ursus maritimus) across

the Arctic. Environmental Research 140:45-55.

23 Douglas, D.C. 2010. : Projected changes in timing and extent of sea ice in

the Bering and Chukchi Seas: U.S. Geological Survey Open-File Report 2010-1176, 32pp.

Durner, G.M., S.C. Amstrup, and K.J. Ambrosius. 2001. Remote identification of polar bear

maternal den habitat in Northern Alaska. Arctic 54(2):115–121.

Durner, G.M., S.C. Amstrup, and K.J. Ambrosius. 2006. Polar bear maternal den habitat in the

Arctic National Wildlife Refuge, Alaska. Arctic 59(1):31–36.

Durner, G.M., D.C. Douglas, R.M. Nielson, S.C. Amstrup, T.L. McDonald, I Stirling, M.

Mauritzen, E.W. Born, Ø. Wiig, E. DeWeaver, M.C. Serreze, S.E. Belikov, M.M.

Holland, J. Maslanik, J. Aars, D.C. Bailey, and A.E. Derocher. 2009. Predicting 21st

century polar bear habitat distribution from global climate models. Ecological

Monographs 79(1): 25–58.

Durner, G.M., A.S. Fischbach, S.C. Amstrup, and D.C. Douglas. 2010. Catalogue of polar bear

(Ursus maritimus) maternal den locations in the Beaufort Sea and neighboring regions,

Alaska, 1910–2010: U.S. Geological Survey Data Series 568.

Durner, G.M., K. Simac, and S.C. Amstrup. 2013. Mapping Polar Bear Maternal Denning

Habitat in the National Petroleum Reserve - Alaska with an IfSAR Digital Terrain Model.

Arctic 66:197–206.

Durner, G.M., J.P. Whiteman, H.J. Harlow, S.C. Amstrup, E.V. Regehr, and M. Ben-David. 2011.

Consequences of long-distance swimming and travel over deep-water pack ice for a

female polar bear during a year of extreme sea ice retreat. Polar Biology 34:975-984.

Evans, T.J. 2004a. Concentrations of selected essential and non-essential elements in adult male

24 polar bears (Ursus maritimus) from Alaska. U.S. Fish and Wildlife Service Technical

Report. MMM 04-02. 68pp.

Evans, T.J. 2004b. PCBs and chlorinated pesticides in adult male polar bears (Ursus maritimus)

from Alaska. U.S. Fish and Wildlife Service Technical Report. MMM 04-01. 61pp.

Fischbach, A.S., S.C. Amstrup, and D.C. Douglas. 2007. Landward and eastward shift of Alaskan

polar bear denning associated with recent sea ice changes. Polar Biology 30:1395–1405.

Fowler, C., W.J. Emery, and J. Maslanik. 2004. Satellite-derived evolution of Arctic sea ice

age: October 1978 to March 2003. Geoscience and Remote Sensing Letters IEEE

1(2):71–74.

Garner, G.W., S.T. Knick, and D.C. Douglas. 1990. Seasonal movements of adult female polar

bears in the Bering and Chukchi seas. International Conference on Bear Research and

Management 8:219–226.

Garner, G.W., L.L. McDonald, D.S. Robson, D.P. Young Jr., and S.M. Arthur. 1992. Literature

review: population estimation methodologies applicable to the estimation of abundance

of polar bears. Internal Report, USFWS. 102pp.

Garner, G.W., L.L. McDonald, S.M. Arthur, and T.L. Olson. 1994. Operating procedures: Pilot

polar bear survey Beaufort Sea: 1994. Internal Report, USFWS, 39 pp.

Gleason, J.S. and K.D. Rode. 2009. Polar bear distribution and habitat association reflect long-

term changes in fall sea ice conditions in the Alaskan Beaufort Sea. Arctic 62:405–417.

Holland, M., C.M. Bitz, and B. Tremblay. 2006. Future abrupt reductions in summer Arctic sea

ice. Geophysical Research Letters 33:L25503.

25 Hunter, C.M., H. Caswell, M.C. Runge, E.V. Regehr, S.C. Amstrup, and I. Stirling. 2010. Climate

change threatens polar bear populations: a stochastic demographic analysis. Ecology

91:2883–2897.

Johnson, C. 2002. Polar bear co-management in Alaska: Cooperative Management between the

U.S. Fish and Wildlife Service and the native hunters of Alaska for the conservation of

polar bears. In: Lunn, N.J., Schliebe, S., and Born, E., (Eds.), Polar bears: Proceedings of

the 13th Working Meeting of the IUCN/SSC Polar Bear Specialist Group, 23–28 June

2001, Nuuk, Greenland. Occasional Paper of the IUCN Species Survival Commission No.

26 (pp. 139–141). Gland, Switzerland: IUCN.

Joint Secretariat. 2015. Inuvialuit and Nanuq: A Polar Bear Traditional Knowledge Study. Joint

Secretariat, Inuvialuit Settlement Region. 304pp.

Kannan, K., T. Agusa, T.J. Evans, and S. Tanabe. 2007. Trace element concentrations in livers

of polar bears from tow population in northern and western Alaska. Archives of

Environmental Contaminants and Toxicology 53:473–482.

Lentfer, J.W. 1974. Discreteness of Alaskan polar bear populations. Proceedings of the

International Congress of Game Biologists 11:323–329.

Lentfer, J.W. 1976. Environmental contaminants and parasites in polar bears. Alaska

Department of Fish and Game, Pittman-Robertson Project Report. W-17-4 and W-17-5.

22 pp.

Lentfer, J.W. 1983. Alaskan polar bear movements from mark and recovery. Arctic 36:282–

288.

26 Lentfer, J.W., and W.A. Galster. 1987. Mercury in polar bears from Alaska. Journal of Wildlife

Diseases 23:338–341.

Lindsay, R.W., and J. Zhang. 2005. The thinning of the Arctic sea ice, 1988-2003: have we

passed a tipping point? Journal of Climate 18:4879–4894.

Manning, T.H. 1971. Geographical variation in the polar bear Ursus maritimus Phipps.

Canadian Wildlife Service Report Series No. 13. 27 pp.

Malenfant, R.M., C.S. Davis, C.I. Cullingham, D.W. Coltman. DW. 2016. Circumpolar Genetic

Structure and Recent Gene Flow of Polar Bears: A Reanalysis. PLoS ONE 11(3): e0148967.

doi:10.1371/journal. pone.0148967.

McKinney, M.A., R.J. Letcher, J. Aars, E.W. Born, M. Branigan, R. Dietz, T.J. Evans, G.W.

Gabrielsen, E. Peacock, and C. Sonne. 2011. Flame retardants and legacy contaminants

in polar bears from Alaska, Canada, East Greenland, and Svalbard, 2005-2008.

Environmental International 37:365-374.

Nageak, B.P., C.D.N. Brower, and S.L. Schliebe. 1991. Polar bear management in the southern

Beaufort Sea: An Agreement between the Inuvialuit Game Council and the North Slope

Borough Fish and Game Committee. Transactions of North American Wildlife and

Natural Resources Conference. 56:337–343.

National Research Council. 2014. Responding to oil spills in the U.S. Arctic marine

environment. National Academies Press, Washington, D.C.

Obbard, M.E., Thiemann, G.W., Peacock, E., and DeBruyn, T.D. (Eds.). 2010. Polar Bears:

27 Proceedings of the 15th Working Meeting of the IUCN/SSC Polar Bear Specialist Group,

Copenhagen, Denmark, 29 June–3 July 2009. Gland, Switzerland and Cambridge, UK:

IUCN. vii + 235 pp.

Øritsland, N.A., Engelhardt, F.R., Juck, F.A., Hurst, R.J., Watts, P.D., 1981. Effect of crude oil on

polar bears. Indian and Northern Affairs Canada, Ottawa, ON, Canada.

Overland, J.E. and M. Wang. 2013. When will the summer Arctic be nearly sea ice free?

Geophysical Research Letters. 40:2097–2101. doi:10.1002/grl.50316.

Pagano, A.M., G.M. Durner, S.C. Amstrup, K.S. Simac, and G.S. York. 2012. Long-distance

swimming by polar bears (Ursus maritimus) of the southern Beaufort Sea during years

of extensive open water. Canadian Journal of Zoology 90:663-676.

Polar Bear Range States. 2015. Circumpolar Action Plan. Conservation Strategy for the Polar

Bear. Available at: http://naalakkersuisut.gl/en/Naalakkersuisut/Departments/Fiskeri-

Fangst-og-Landbrug/Isbjorn/The-Circumpolar-Action-Plan-and-Executive-Summary.

[Accessed 31 July 2016]

Polar Bear Specialist Group (PBSG). 2015. Status Table of the PBSG. Available at:

http://pbsg.npolar.no/en/status/status-table.html . [Accessed 30 November 2015].

Peacock, E., M.K. Taylor, J. Laake, and I. Stirling. 2013. Population ecology of polar bears in

Davis Strait, Canada and Greenland. Journal of Wildlife Management 77:463–476.

Peacock, E., S.A. Sonsthagen, M.E. Obbard, A. Boltunov, E.V. Regehr, N. Ovsyanikov, J. Aars,

S.N. Atkinson, G.K. Sage, A.G. Hope, E. Zeyl, L. Bachmann, D. Ehrich, K.T. Scribner,

S.C. Amstrup, S. Belikov, E.W. Born, A.E. Derocher, I. Stirling, M.K. Taylor, Ø. Wiig,

28

D. Paetkau, and S.L. Talbot. 2015. Implications of the Circumpolar Genetic Structure of

Polar Bears for Their Conservation in a Rapidly Warming Arctic. PLoS One 10:

e0136126.

Paetkau, D., S.C. Amstrup, E.W. Born, W. Calvert, A.E. Derocher, G.W. Garner, F. Messier, I.

Stirling, M.K. Taylor, Ø. Wiig, and C. Strobeck. 1999. Genetic Structure of the world’s

polar bear populations. Molecular Ecology 8:1571–1584.

Parkinson, C.L., D.J. Cavalieri, P. Gloersen, H.J. Zwally, and J.C. Comiso. 1999. Arctic sea ice

extents, areas, and trends, 1978–1996. Journal of Geophysical Research 104(C9):20837–

20856.

Prestrud, P. and I. Stirling. 1994. The international polar bear agreement and the current status

of polar bear conservation. Aquatic Mammals 20:113–124.

Regehr, E.V., S.C. Amstrup, and I. Stirling. 2006. Polar bear population status in the southern

Beaufort Sea. U.S. Geological Survey Open File Report 2006-1337. 20 pp.

Regehr, E.V., N.J. Lunn, S.C. Amstrup, and I. Stirling. 2007. Effects of earlier sea ice breakup on survival and population size of polar bears in western . Journal of

Wildlife Management 71:2673–2683.

Regehr, E.V., C.M. Hunter, H. Caswell, S.C. Amstrup, and I. Stirling. 2010. Survival and

breeding of polar bears in the southern Beaufort Sea in relation to sea ice. Journal of

Animal Ecology 79:117–127.

Regehr, E.V., R.R. Wilson, K.D. Rode, and M.C. Runge. 2015. Resilience and risk—A

demographic model to inform conservation planning for polar bears: U.S. Geological

29 Survey Open-File Report 2015-1029. 56 p. http://dx.doi.org/10.3133/ofr20151029.

Rode, K.D., S.C. Amstrup, and E.V. Regehr. 2010. Reduced body size and cub recruitment

associated with sea ice decline in polar bears. Ecological Applications 20:768–782.

Rode, K.D., E.V. Regehr, D.C. Douglas, G. Durner, A.E. Derocher, G.W. Thiemann, and S.M.

Budge. 2014. Variation in the response of an Arctic top predator experiencing habitat

loss: feeding and reproductive ecology of two polar bear populations. Global Change

Biology 20:76–88.

Rode, K.D., R.R. Wilson, E.V. Regehr, M. St. Martin, D.C. Douglas, and J. Olson. 2015.

Increased Land Use by Chukchi Sea Polar Bears in Relation to Changing Sea Ice

Conditions. PLoS ONE 10(11): e0142213. doi:10.1371/journal.pone.0142213.

Rothrock, D.A., Y. Yu, and G.A. Maykut. 1999. Thinning of the Arctic sea-ice cover,

Geophysical Research Letters 26:3469–3472.

Routti, H., R.J. Letcher, E.W. Born, M. Branigan, R. Dietz, T.J. Evans, A.T. Fisk, E. Peacock,

C. Sonne. 2011. Spatial and temporal trends of selected trace elements in liver tissue from

polar bears (Ursus maritimus) from Alaska, Canada, and Greenland. Journal of

Environmental Monitoring 8:2260-2267.

Schliebe, S., T. Evans, K. Johnson, M. Roy, S. Miller, C. Hamilton, R. Meehan, and S.

Jahrsdoerfer. 2006. Range-wide status review of the polar bear (Ursus maritimus). U.S.

Fish and Wildlife Service, Anchorage, Alaska, USA.

Schliebe, S., K.D. Rode, J.S. Gleason, J. Wilder, K. Proffitt, T.J. Evans, and S. Miller. 2008.

Effects of sea ice extent and food availability on spatial and temporal distribution of polar

30 bears during the fall open-water period in the Southern Beaufort Sea. Polar Biology

12:999–1010.

Scribner, K.T., G.W. Garner, S.C. Amstrup, and M.A. Cronin. 1997. Population genetic studies

of the Polar Bear (Ursus maritimus): a summary of available data and interpretation of

results. In: S. Dizon, J. Chivers, and W. Perrin, (Eds.), Molecular genetics of marine

mammals, incorporating the proceedings of a workshop on the analysis of genetic data to

address problems of stock identity as related to management of marine mammals.

Special Publication #3 of the Society of Marine Mammalogy (pp. 185–196).

Serreze, M.C., M.M. Holland, and J. Stroeve. 2007. Perspectives on the Arctic’s shrinking sea-

ice cover. Science 315:1533–1536.

Smith, L. C. and S. R. Stephenson. 2013. New Trans-Arctic shipping routes navigable by

midcentury, Proc. Nat. Acad. Sci., 110(13), E1191–E1195,

doi:10.1073/pnas.1214212110.

St. Aubin, D.J. 1990. Physiologic and toxic effects on polar bears. In: J.R. Geraci and D.J. St.

Aubin, (Eds.), Sea mammals and oil: confronting the risks (pp. 235–239). Academic

Press, Inc. New York, New York, USA.

Stirling, I. and Derocher, A.E. 2012. Effects of climate warming on polar bears: a review of the

evidence. Global Change Biology. 18.2694-2706. doi:10.1111/j.1365-2486.2012.02753.x.

Stirling, I. and C.L. Parkinson. 2006. Possible effects of climate warming on selected

populations of polar bears (Ursus maritimus) in the Canadian Arctic. Arctic 99(3):261–

275.

31 Stirling, I, T.L. McDonald, E.S. Richardson, and E.V. Regehr. 2007. Polar bear population

status in the Northern Beaufort Sea. U.S. Geological Survey, Alaska Science Center,

Administrative Report 31 pp.

Stirling, I., T.L. McDonald, E.S. Richardson, E.V. Regehr, and S.C. Amstrup. 2011. Polar bear

population status in the northern Beaufort Sea, Canada, 1971–2006. Ecological

Applications 21:859–876.

Stroeve, J., M. Serreze, S. Drobot, S. Gearheard, M. Holland, J. Maslanik, W. Meier, and T.

Scambos. 2008. Arctic Sea Ice Extent Plummets in 2007. Transactions of the American

Geophysical Union 89(2):13–14.

Stroeve, J.C., V. Kattsov, A. Barrett, M. Serreze, T. Pavlova, M. Holland, and W.N. Meier.

2012. Trends in Arctic sea ice extent from CMIP5, CMIP3 and observations.

Geophysical Research Letters 39:L16502.

Stroeve, J.C., T. Markus, L. Boisvert, J. Miller, and A. Barrett. 2014. Changes in Arctic melt

season and implications for sea ice loss. Geophysical Research Letters 41:1216–1225.

Thiemann, G.W., S.J. Iverson, and I. Stirling. 2008. Polar bear diets and arctic marine food webs:

Insights from fatty acid analysis. Ecological Monographs 78:591–613.

Treseder, L. and A. Carpenter. 1989. Polar bear management in the Southern Beaufort Sea.

Information North 15(4):2–4.

U.S. Fish and Wildlife Service (USFWS). 2011. Summary of polar bear management in Alaska

2009/2010: Report to the Canadian Polar Bear Technical Committee February 1–3, 2011.

Winnipeg, Manitoba, Canada.

32 U.S. Geological Service (USGS). Unpublished data (research data). Available from:

USGS/Alaska Science Center, 4210 University Drive, Anchorage, Alaska 99508.

Wade, P. R. 1998. Calculating thresholds to the human-caused mortality of cetaceans and

pinnipeds. Marine Mammal Science, 14: 1–37.

Wade, P.R., and R. Angliss. 1997. Guidelines for assessing marine mammal stocks: Report in

the GAMMS Workshop, April 3–5, 1996, Seattle, Washington. 93pp.

Wilson, D.E. 1976. Cranial variation in polar bears. International Conference Bear Research

and Management 3:447–453.

33

Figure 1. Map of the polar bear subpopulations: Southern Beaufort Sea (SB), Chukchi Sea,

Laptev Sea, , , East Greenland, Northern Beaufort (NB), Kane Basin (KB),

Norwegian Bay (NW), Lancaster Sound (LS), (GB), McClintock Channel (MC),

Viscount Melville (VM), , , , Western Hudson Bay (WH), and

Southern Hudson Bay (source: Polar Bear Specialist Group: http://pbsg.npolar.no/en/status/population-map.html).

34

Figure 2. Approximate distribution of polar bears (the Southern Beaufort Sea, Northern

Beaufort Sea, and Chukchi/ polar bear stocks) in Alaska. Distributions are based on the 95% annual contours of utilization distributions developed from 1985 to 2003 satellite- collar data for the Southern Beaufort and Chukchi/Bering Sea stocks, and 1989-1991 for the

Northern Beaufort Sea stock (Amstrup et. al 2005).

35

33

25 25

18 18 17 17 15 12

9

Figure 3. Polar bear harvest in the U.S. portion of the Southern Beaufort Sea stock, 2006-2015.

36